One reason is because there is very little water vapor. The other is because air in the stratosphere is stable. This means that there is no inherent tendency for it to rise, since temperature increases with altitude.
The air pressure in the stratosphere is low. This layer of the atmosphere is located above the troposphere where most of Earth's weather occurs, so it has less air concentration and lower pressure as you move higher in altitude.
The air pressure at the top of the stratosphere is very low, around 0.1 millibars, which is much lower than at the Earth's surface. It is where the Earth's atmosphere thins out and merges with space.
As you move from the troposphere to the stratosphere, the temperature typically increases due to the presence of the ozone layer which absorbs UV radiation. In the stratosphere, the jet stream and most weather phenomena occur, making it a region of significant atmospheric stability and less turbulence compared to the troposphere below.
The air pressure in the mesosphere is extremely low, typically less than 0.1% of the pressure at sea level. This region of the atmosphere is located between the stratosphere and thermosphere, with pressures decreasing significantly with altitude.
Air from the troposphere and stratosphere doesn't mix freely because of a layer called the tropopause, which acts as a barrier preventing the two layers from easily intermingling. The tropopause has different temperature and pressure characteristics that act as a boundary between the troposphere and stratosphere. This separation helps maintain the stability and structure of each layer.
Air pressure decreases as you move from the troposphere to the stratosphere. This is because the weight of the air above is less in the stratosphere, leading to lower air pressure at higher altitudes.
air pressure decreases
Yes, the stratosphere has lower air pressure compared to the troposphere, which is the layer of the atmosphere closest to the Earth's surface. As altitude increases in the stratosphere, air pressure decreases due to the reduced density of air molecules. This lower pressure affects various atmospheric phenomena, including weather patterns and the behavior of aircraft.
Low
About 1 millibar.
The air pressure in the stratosphere is low. This layer of the atmosphere is located above the troposphere where most of Earth's weather occurs, so it has less air concentration and lower pressure as you move higher in altitude.
In the stratosphere, air pressure typically ranges from about 1000 millibars at the bottom to around 100 millibars at the top, which is approximately 50 kilometers (31 miles) above the Earth's surface. The pressure decreases with altitude due to the thinning of the atmosphere. As you ascend through the stratosphere, the air becomes less dense, resulting in lower pressure.
The air pressure at the top of the stratosphere is very low, around 0.1 millibars, which is much lower than at the Earth's surface. It is where the Earth's atmosphere thins out and merges with space.
As you move from the troposphere to the stratosphere, the temperature typically increases due to the presence of the ozone layer which absorbs UV radiation. In the stratosphere, the jet stream and most weather phenomena occur, making it a region of significant atmospheric stability and less turbulence compared to the troposphere below.
Air pressure in the stratosphere decreases with altitude, starting at about 1,000 hPa (hectopascals) at the boundary with the troposphere and dropping to around 100 hPa at the stratopause, which is approximately 50 kilometers (31 miles) above Earth's surface. The stratosphere is characterized by a temperature inversion, where temperature increases with altitude, which affects the behavior of air pressure. Overall, the stratospheric pressure is much lower than that at sea level due to the reduced density of air at higher elevations.
The air pressure in the mesosphere is extremely low, typically less than 0.1% of the pressure at sea level. This region of the atmosphere is located between the stratosphere and thermosphere, with pressures decreasing significantly with altitude.
No, the stratosphere does not contain enough air for living things to breathe. Most of the Earth's breathable air is found in the troposphere, the layer of the atmosphere closest to the Earth's surface, where weather occurs and where oxygen is abundant. The stratosphere, while it contains some air, has much lower pressure and oxygen levels, making it inhospitable for life as we know it.